Dependence of the Timing of Hydrogeochemical Earthquake Precursor in the Southern Baikal Area on the Energy Classes of the Earthquakes and Their Epicentral Distances


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Abstract

Data obtained on dissolved He concentrations in the waters of blowing wells in the southern Baikal area indicate that these concentrations show certain variations on the eve of earthquakes. Based on these data, a correlation dependence was calculated for the function log τR (logarithm of the product of the precursor time of a seismic event by its epicentral distance) on the energy class of the earthquake. Variations in the He concentrations are suggested to be viewed as a short-term precursor of earthquakes.

About the authors

R. M. Semenov

Institute of the Earth’s Crust, Siberian Division, Russian Academy of Sciences; Irkutsk State University of Transport Routes

Author for correspondence.
Email: semenov@crust.irk.ru
Russian Federation, Irkutsk, 664033; Irkutsk, 664074

M. N. Lopatin

Irkutsk State University; Urangeologorazvedka JSC, Sosnovgeologiya PA

Author for correspondence.
Email: flamewolf@mail.ru
Russian Federation, Irkutsk, 664033; Irkutsk, 664039

V. V. Chechel’nitskii

Baikal Branch, Federal Research Center, Geophysical Survey, Russian Academy of Sciences

Author for correspondence.
Email: chechel@crust.itk.ru
Russian Federation, Irkutsk, 664033

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